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Perspective on the Tidal Bore: Background and Initiation
Volume 1: Symposia, Parts A and B, 2012Tidal bores have been the subject or cause of legend, poetry, recreation, tourism, shipping disasters, and scientific interest for centuries. They pose interesting theoretical questions for the engineer. Introductory details are presented regarding the remarkable tidal bore phenomenon, including discussion of the tidal bore in various locations and a ...
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Internal tidal bores and bottom nepheloid layers
Continental Shelf Research, 2001Abstract During a littoral optical environment project field study in shallow water off Oceanside, California, large spikes in optical attenuation (dominated by suspended particles) were observed in a near-bottom mooring. Using moored current meters together with aircraft remote imaging overflights and profiling anchor stations, we established that ...
Donald R. Johnson +2 more
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Tidal Bores, Aegir, Eagre, Mascaret, Pororoca [PDF]
A tidal bore is a series of waves propagating upstream as the tidal flow turns to rising. It forms during spring tide conditions when the tidal range exceeds 4 to 6 m and the flood tide is confined to a narrow funnelled estuary. Its existence is based upon a fragile hydrodynamic balance between the tidal amplitude, the freshwater river flow conditions ...
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Mixing and Dispersion in Tidal Bores: A Review [PDF]
When a river mouth has a flat converging shape and when the tidal range exceeds 6 to 9 m, the river may experience a tidal bore. A tidal bore is basically a positive surge propagating upstream as the tidal flow turns to rising. The occurrence of a bore has a significant impact on estuarine systems.
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CFD modeling of tidal bores: development and validation challenges
Coastal Engineering Journal, 2018Xinqian Leng +2 more
exaly
Internal tidal bores in the Monterey Canyon
2012A thirty-four day record of near-bottom temperature and horizontal velocity spanning the lower third of the water column from within Monterey Canyon was examined. The observed internal tide is highly non-linear with kinetic energy dispersed among numerous overtides near the bottom and more concentrated in the primary semi diurnal constituent (M2 ...
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